FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2951818431> ?p ?o ?g. }

• W2951818431 endingPage "103889" @default.
• W2951818431 startingPage "103889" @default.
• W2951818431 abstract "Abstract Mineral chemistry, petrography and crystal size distributions of Early Miocene mafic and intermediate lavas from the Kepsut Volcanic Complex (KVC) have been studied to decipher magma chamber processes and dynamics beneath northwestern Anatolia. KVC which is a part of the Western Anatolian Volcanic Province comprises lavas represented by various compositions ranging from basaltic andesite to rhyodacite and associated pyroclastics. Basaltic andesite and andesite lavas of the KVC, the focus of this study, present distinct petrographical features such as three plagioclase generations, patchy zoning, oscillatory reverse zoning, sieve textured crystals and clinopyroxene-mantled amphibole that are clear indicators of disequilibrium conditions in magma chamber(s). Petrography, mineral chemistry and crystal size distribution studies of andesite and basaltic andesite lavas of the KVC indicate that magma evolution occurred in four stages: (I) Near-Equilibrium Stage, (II) Mafic Input Stage, (III) Mixing/Mingling Stage and (IV) Pre-eruption Stage. Thermobarometry calculations indicate that crystallization of andesite and basaltic lavas occurred at similar pressure (mid-to-deep crustal depths, 5–7 kbar) but distinct temperature conditions (920–952 °C and 921–1069 °C, respectively) suggesting that KVC magmas evolved either in the same or different magma chambers at similar depths and experienced open-system processes. Both of these hypotheses are compatible with multistage evolution of the KVC. Combined petrography, mineral chemistry and geothermometry studies on KVC rocks indicate that mixing/mingling processes and subsequent decompression-driven crystallization were the principal mechanisms for the origin of the textural and mineralogical diversity that is characteristic of KVC lavas. Disequilibrium crystallization was probably caused by the influx of a hotter basaltic magma into crustal magma chambers during the first major period of north-south extension in western Anatolia." @default.
• W2951818431 created "2019-06-27" @default.
• W2951818431 creator A5034348994 @default.
• W2951818431 creator A5064481881 @default.
• W2951818431 date "2019-09-01" @default.
• W2951818431 modified "2023-10-17" @default.
• W2951818431 title "Magma chamber processes and dynamics beneath northwestern Anatolia: Insights from mineral chemistry and crystal size distributions (CSDs) of the Kepsut volcanic complex (NW Turkey)" @default.
• W2951818431 cites W1485237895 @default.
• W2951818431 cites W1485617499 @default.
• W2951818431 cites W1966987822 @default.
• W2951818431 cites W1968681946 @default.
• W2951818431 cites W1971941121 @default.
• W2951818431 cites W1978262868 @default.
• W2951818431 cites W1978533876 @default.
• W2951818431 cites W1980254060 @default.
• W2951818431 cites W1989491939 @default.
• W2951818431 cites W1991521847 @default.
• W2951818431 cites W1994919247 @default.
• W2951818431 cites W2003279842 @default.
• W2951818431 cites W2014333968 @default.
• W2951818431 cites W2016987673 @default.
• W2951818431 cites W2019877001 @default.
• W2951818431 cites W2032208445 @default.
• W2951818431 cites W2032975081 @default.
• W2951818431 cites W2033034443 @default.
• W2951818431 cites W2039239326 @default.
• W2951818431 cites W2040092205 @default.
• W2951818431 cites W2040549377 @default.
• W2951818431 cites W2043853147 @default.
• W2951818431 cites W2045769202 @default.
• W2951818431 cites W2046345979 @default.
• W2951818431 cites W2069682878 @default.
• W2951818431 cites W2077216152 @default.
• W2951818431 cites W2077938222 @default.
• W2951818431 cites W2078446859 @default.
• W2951818431 cites W2083569297 @default.
• W2951818431 cites W2085045756 @default.
• W2951818431 cites W2087292109 @default.
• W2951818431 cites W2088599153 @default.
• W2951818431 cites W2091191350 @default.
• W2951818431 cites W2095601024 @default.
• W2951818431 cites W2095893599 @default.
• W2951818431 cites W2104883999 @default.
• W2951818431 cites W2119691316 @default.
• W2951818431 cites W2123698291 @default.
• W2951818431 cites W2167383526 @default.
• W2951818431 cites W2208975454 @default.
• W2951818431 cites W2236545372 @default.
• W2951818431 cites W2735201426 @default.
• W2951818431 cites W2765090629 @default.
• W2951818431 cites W2884064230 @default.
• W2951818431 cites W2890199008 @default.
• W2951818431 cites W2944056967 @default.
• W2951818431 cites W2944757286 @default.
• W2951818431 cites W83058367 @default.
• W2951818431 doi "https://doi.org/10.1016/j.jseaes.2019.103889" @default.
• W2951818431 hasPublicationYear "2019" @default.
• W2951818431 type Work @default.
• W2951818431 sameAs 2951818431 @default.
• W2951818431 citedByCount "7" @default.
• W2951818431 countsByYear W29518184312019 @default.
• W2951818431 countsByYear W29518184312020 @default.
• W2951818431 countsByYear W29518184312021 @default.
• W2951818431 countsByYear W29518184312022 @default.
• W2951818431 crossrefType "journal-article" @default.
• W2951818431 hasAuthorship W2951818431A5034348994 @default.
• W2951818431 hasAuthorship W2951818431A5064481881 @default.
• W2951818431 hasConcept C120806208 @default.
• W2951818431 hasConcept C127313418 @default.
• W2951818431 hasConcept C17409809 @default.
• W2951818431 hasConcept C183222429 @default.
• W2951818431 hasConcept C191897082 @default.
• W2951818431 hasConcept C192562407 @default.
• W2951818431 hasConcept C1965285 @default.
• W2951818431 hasConcept C199289684 @default.
• W2951818431 hasConcept C2776432453 @default.
• W2951818431 hasConcept C5900021 @default.
• W2951818431 hasConcept C9566828 @default.
• W2951818431 hasConceptScore W2951818431C120806208 @default.
• W2951818431 hasConceptScore W2951818431C127313418 @default.
• W2951818431 hasConceptScore W2951818431C17409809 @default.
• W2951818431 hasConceptScore W2951818431C183222429 @default.
• W2951818431 hasConceptScore W2951818431C191897082 @default.
• W2951818431 hasConceptScore W2951818431C192562407 @default.
• W2951818431 hasConceptScore W2951818431C1965285 @default.
• W2951818431 hasConceptScore W2951818431C199289684 @default.
• W2951818431 hasConceptScore W2951818431C2776432453 @default.
• W2951818431 hasConceptScore W2951818431C5900021 @default.
• W2951818431 hasConceptScore W2951818431C9566828 @default.
• W2951818431 hasFunder F4320324489 @default.
• W2951818431 hasLocation W29518184311 @default.
• W2951818431 hasOpenAccess W2951818431 @default.
• W2951818431 hasPrimaryLocation W29518184311 @default.
• W2951818431 hasRelatedWork W1965128824 @default.
• W2951818431 hasRelatedWork W2003541641 @default.
• W2951818431 hasRelatedWork W2021308518 @default.
• W2951818431 hasRelatedWork W2022811445 @default.
• W2951818431 hasRelatedWork W2027913588 @default.

• next